0.95
vhm149 1.46
vhm205 1.01
vhm206 1.28
vhm221 0.9
vhm265 1.16
vhm277 0.87
vhm278 -0.12
18
l
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−2 0 2 4 6
0
1
2
3
4
−ln(−ln(1−1/T))
Q/
E[
Q]
1 2 5 10 20 50 100
T (years)
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l
l
l
l
l
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l
vhm148
vhm149
vhm205
vhm206
vhm221
vhm265
vhm277
vhm278
Regional +/− 95% CI
H1 0.995
H2 −0.877
l
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l l l l
l
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l l
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/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf
20
0
60
0
J F M A M J J A S O N D
0
20
0
60
0
J F M A M J J A S O N D
0
50
10
0
15
0
J F M A M J J A S O N D
0
50
10
0
15
0
J F M A M J J A S O N D
0
10
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0
J F M A M J J A S O N D
0
10
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30
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J F M A M J J A S O N D
0
40
0
80
0
120
0
J F M A M J J A S O N D
0
40
0
80
0
120
0
J F M A M J J A S O N D
0
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80
12
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J F M A M J J A S O N D
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12
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J F M A M J J A S O N D
/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
scale, used to identify weather analogues. These fields are
extracted twice daily (00UTC and 12UTC) on a 1 x 1 latitude-longitude grid from the
ECMWF operational analysis and forecasts available for the period 2001–2006. The ana-
logue meteorological situations are extracted from the ERA-40 reanalysis archive (Uppala
et al., 2005) for the period 1958–2001.
14
Predictants:
Gridded series of daily
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf